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Probability distribution of groundcover for runoff prediction in rangeland in the Burnett-Mary Region, Queensland

机译:昆士兰伯特玛丽地区牧场地下铺地区地下筹馆的概率分布

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摘要

Considering the degree of spatial and temporal variation of groundcover in grazing land, it is desirable to use a simple and robust model to represent the spatial variation in cover in order to quantify its effect on runoff and soil loss. The purpose of the study was to test whether a two-parameter beta (beta) distribution could be used to characterise cover variation in space at the sub-catchment scale. Twenty sub-catchments (area range 35.8-231 km(2)) in the Burnett Mary region, Queensland, were randomly selected. Thirty raster layers of groundcover at 30-m resolution were prepared for these 20 sub-catchments with the average cover for the 30 layers ranging from 24% to 91%. Three methods were used to test the appropriateness of the beta distribution for characterising the cover variation in space: (i) visual goodness-of-fit assessment and Kolmogorov-Smimov (K-S) test; (ii) the fractional area with cover <= 53%; and (iii) estimated runoff amount for a given rainfall amount for the area with cover <= 53%. The K-S test on 30 x 100 samples of groundcover showed that the hypothesis of beta distribution for groundcover could not be rejected at P = 0.05 for 97.5% of the cases. A comparison of the observed and beta distributions in terms of the fractional area with cover <= 53% showed that the discrepancy <= 8% was for the 30 layers considered. A comparison in terms of the estimated runoff showed that results using the observed cover distribution and the beta distribution were highly correlated (R-2 range 0.91-0.98; Nash-Sutcliffe efficiency measure range 0.88-0.99). The mean absolute error of estimated runoff ranged from 0.98 to 8.10 mm and the error relative to the mean was 4-16%. The results indicated that the two-parameter beta distribution can be adequately used to characterise the spatial variation of cover and to evaluate the effect of cover on runoff for these predominantly grazing catchments.
机译:考虑到地面覆盖土地上的地基的空间和时间变化程度,希望使用简单且鲁棒的模型来表示盖子的空间变化,以便量化其对径流和土壤损失的影响。该研究的目的是测试双参数β(Beta)分布是否可用于在子集型秤上表征空间的覆盖变化。在昆士兰伯特玛丽地区的二十个子集水区(面积范围35.8-231km(2))被随机选择。对于这些20个分辨率的30米分辨率的三十栅格层,对于30层的平均覆盖物,通常为24%至91%。三种方法用于测试β分布的适当性,用于表征空间的覆盖变化:(i)视觉良好的拟合评估和Kolmogorov-Smimov(K-S)测试; (ii)具有封面的分数区域<= 53%; (iii)覆盖覆盖区域的给定降雨量的估计径流金额<= 53%。在30×100个地下面的K-S试验表明,地下截断的β分布的假设不能在P = 0.05中被拒绝97.5%。观察到的和β分布在具有封面的分数区域的比较<= 53%表示差异<= 8%用于考虑的30层。在估计的径流方面的比较显示,使用观察到的覆盖分布和β分布的结果高度相关(R-2范围0.91-0.98;纳什 - Sutcliffe效率测量范围0.88-0.99)。估计径流的平均绝对误差范围为0.98至8.10毫米,相对于平均值的误差为4-16%。结果表明,两参数β发布可以充​​分用于表征盖子的空间变化,并评估覆盖覆盖对这些主要放牧液集的影响。

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